The subterranean or underground rivers of London are or were the direct or indirect tributaries of the upper estuary of the Thames that were built over during the growth of the metropolis of London. They now flow through culverts, with some of them integral parts of London's sewerage system and diverted accordingly.
Subterranean London refers to a number of subterranean structures that lie beneath London. The city has been occupied by humans for two millennia. Over time, the capital has acquired a vast number of these structures and spaces, often as a result of war and conflict.
The River Fleet is the largest of London's subterranean rivers, all of which today contain foul water for treatment. It has been used as a sewer since the development of Joseph Bazalgette's London sewer system in the mid-19th century with the water being treated at Beckton Sewage Treatment Works. Its headwaters are two streams on Hampstead Heath, each of which was dammed into a series of ponds—the Hampstead Ponds and the Highgate Ponds—in the 18th century. At the southern edge of Hampstead Heath these descend underground as sewers and join in Camden Town. The waters flow 4 miles (6 km) from the ponds.
The River Effra is a former set of streams in south London, England, culverted and used mainly for storm sewerage. It had been a tributary of the Thames. Its catchment waters, where not drained to aquifer soakaways and surface water drains, have been incorporated into 1850s-built combined sewer sectors, devised by Sir Joseph Bazalgette. One drains Peckham, the other Brixton, then intended to flow towards Peckham. These generally flow east to be treated at Crossness.
The Westbourne or Kilburn is a culverted small River Thames tributary in London, rising in Hampstead and Brondesbury Park and which as a drain unites and flows southward through Kilburn and Bayswater to skirt underneath the east of Hyde Park's Serpentine lake then through central Chelsea under Sloane Square. It passes centrally under the south side of Royal Hospital Chelsea's Ranelagh Gardens before discharging into Inner London's old-fashioned, but grandiose combined sewer system, with exceptional discharges into the Inner London Tideway. Since the latter 19th century, the population of its catchment has risen further but to reduce the toll it places on the Beckton Sewage Treatment Works and related bills its narrow basin has been assisted by private soakaways, and public surface water drains. Its depression has been replaced with and adopted as a reliable route for a gravity combined sewer. The formation of the Serpentine relied on the water, a lake with a long, ornate footbridge and various activities associated, which today uses little-polluted water from a great depth.
The River Wandle is a right-bank tributary of the River Thames in south London, England. With a total length of about 9 miles (14 km), the river passes through the London boroughs of Croydon, Sutton, Merton and Wandsworth, where it reaches the Thames. A short headwater – the Caterham Bourne – is partially in Surrey, the historic county of the river's catchment. Tributaries of the Wandle include Carshalton Ponds and Norbury Brook.
The Colne is a river and a tributary of the River Thames in England. Just over half its course is in south Hertfordshire. Downstream, it forms the boundary between Buckinghamshire and the London Borough of Hillingdon. The confluence with the River Thames is on the Staines reach at Staines-upon-Thames.
The Northern Outfall Sewer (NOS) is a major gravity sewer which runs from Wick Lane in Hackney to the Beckton Sewage Treatment Works in east London. Most of it was designed by Joseph Bazalgette, as a result of an outbreak of cholera in 1853 and the "Great Stink" of 1858.
Tyburn Brook was a small tributary stream to the West Bourne or Westbourne and ran mainly in Hyde Park for a few hundred metres south by south-west. It has lost its catchment to natural drainage into the gravelly topsoil and to surface water, foul and in early Victorian style combined sewers and its small collect, its source remains beneath the earth to feed into a mixture of these. The Serpentine, having been the Westbourne's main showing is now fed by three boreholes instead. It is not to be confused with the much longer Tyburn, Ty Bourne or River Tyburn, but frequently was confused until the early 19th century as both were well west of the walls of the City of London.
Stamford Brook was a tributary of the Tideway stretch of the River Thames in west London supplied by three headwaters. Historically used as an irrigation ditch or dyke, the network of small watercourses had four lower courses and mouths.
Counter's Creek, ending in Chelsea Creek, the lowest part of which still exists, was a stream that flowed from Kensal Green, by North Kensington and flowed south into the River Thames on the Tideway at Sands End, Fulham. Its remaining open watercourse is the quay of Chelsea Creek.
The River Crane, a tributary of the River Thames, runs 8.5 miles (13.6 km) in West London, England. It forms the lower course of Yeading Brook. It adjoins or passes through three London boroughs: Hillingdon, Hounslow and Richmond upon Thames, in the historic county of Middlesex. The drainage basin is heavily urbanised but many of the Hayes to Whitton flood-meadows have been conserved, forming a narrow, green vale, opening out to what remains of Hounslow Heath in the centre – a near-continuous belt of semi-natural habitat.
The River Ash is a small, shallow river in Surrey, England. Its course of 10 kilometres (6.2 mi) is just outside Greater London. Work has been carried out to re-align, clear and build up a small, Littleton head of water and create two backwaters. One backwater dates to the medieval period; the other to the 1990s. It flows as one of the six distributaries of the River Colne from the south of Staines Moor immediately south of the Staines Bypass eastwards through the rest of the borough of Spelthorne before meeting the River Thames.
The Falconbrook was a stream that rose in Balham and Tooting, draining much of those parishes then the south and west of the larger district of Battersea including Clapham Junction to enter the London reaches of the Thames. Before doing so, it briefly formed the border of Wandsworth Town, reflected in the SW11/SW18 boundary today.
Marylebone is an area in London, England and is located in the City of Westminster. It is in Central London and part of the West End. Oxford Street forms its southern boundary.
Minetta Creek was one of the largest natural watercourses in Manhattan, New York City, United States. Minetta Creek was fed from two tributaries, one originating at Fifth Avenue and 21st Street, and the other originating at Sixth Avenue and 16th Street. They joined near Fifth Avenue and 11th Street then took a southwesterly course. Minetta Creek's name is thought to have originated from either the Native American term "Manette", meaning "Devil's Water", or the Dutch word "Minnetje", meaning "the little one".
Sudbrook and its tributary, the Latchmere stream, are north-flowing streams in London, England, that drain northern Kingston upon Thames and the eastern extreme of Ham following a meander scar in a terrace; the upper part of the Sudbrook drains a narrow vale in Richmond Park's southern corner into the tidal Thames.
Eia or Eye was an early Medieval manor in Westminster, Middlesex and is now a part of Central London. It was about one mile west of the Palace of Westminster/Whitehall, about 2 miles west-south-west of the walled City of London, and about half a mile north of the River Thames.
Marylebone Lane is one of the original streets of the Marylebone district of the City of Westminster, London. It runs from Oxford Street in the south to Marylebone High Street in the north, its winding shape following the course of the River Tyburn that it once ran alongside and pre-dating the grid pattern of the other streets in the area. Today the lane is largely composed of small shops, cafes and restaurants with some small apartment blocks. There are some larger commercial buildings at the southern end near Oxford Street.
